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Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. http://geoweb.mit.edu/~ tah [email protected]

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Page 1: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

Applications of the Global Positioning System

Prof. Thomas Herring

Department of Earth, Atmosphere and Planetary Sciences

12.080 Seminar Fall 2004.

http://geoweb.mit.edu/~tah

[email protected]

Page 2: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 2

Overview

• Briefly review history of GPS: original aims of few-meter positioning

• Examine some MIT projects where GPS is used to make sub-millimeter position measurements and study deformation processes.– New Zealand– Oil field deformation– North America Plate deformation

Page 3: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 3

GPS Original Design (circa 1970)

• Started development in the late 1960s as NAVY/USAF project to replace Doppler positioning system

• Aim: Real-time positioning to < 10 meters, capable of being used on fast moving vehicles.

• Limit civilian (“non-authorized”) users to 100 meter positioning.

Page 4: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 4

GPS Design• Innovations:

– Use multiple satellites (originally 21, now ~28)– All satellites transmit at same frequency– Signals encoded with unique “bi-phase,

quadrature code” generated by pseudo-random sequence (designated by PRN, PR number): Spread-spectrum transmission.

– Dual frequency band transmission (allows propagation delay due to the ionosphere to be removed):• L1 ~1.5 GHz, L2 ~1.25 GHz

– Use of phase measurements allows millimeter level position determinations

Page 5: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 5

Latest Block IIR satellite(1,100 kg)

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

• Total system cost is over $10B • Average cost per satellite is

~$60M• None of these costs are passed

directly to users.• Satellites transmit signals that

any one with the correct receivers can use (no use tax on receivers)

Page 6: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 6

Measurements• Measurements:

– Time difference between signal transmission from satellite and its arrival at ground station (called “pseudo-range”, precise to 0.1–10 m)

– Carrier phase difference between transmitter and receiver (precise to a few millimeters)

– Doppler shift of received signal• All measurements relative to “clocks” in ground

receiver and satellites (but use of multiple satellites and receivers allow this problem to be removed).

• High precision, dual frequency receivers now $4000-$6000

Page 7: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 7

Satellite constellation

• Since multiple satellites need to be seen at same time (four or more):– Many satellites (original 21 but now 28)– High altitude so that large portion of Earth

can be seen (20,000 km altitude —MEO)

Page 8: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 8

Current constellation

• Relative sizes correct (inertial space view)

• “Fuzzy” lines not due to orbit perturbations, but due to satellites being in 6-planes at 55o inclination.

Page 9: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 9

Some MIT projects using GPS

• The MIT Geodesy and Geodynamics group (http://geoweb.mit.edu) is involved in many projects around the world with using GPS.

• Three projects to discuss (all involving measurement of height changes)– Uplift in New Zealand Southern Alps– Subsidence in oil fields– Uplift and subsidence across North America (response to

last ice-age: Glacial Isostatic Adjustment GIA)• All these projects involve collaborations with other groups.

Page 10: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 10

A Direct Geodetic Measurement of the Uplift Rate of the Southern Alps

John Beavan1

Mikael Denham2

Paul Denys2

Brad Hager3

Tom Herring3

Chuck Kurnik4

Dion Matheson1

Peter Molnar5

Chris Pearson2

1 GNS2 Otago University3 MIT4 UNAVCO5 Univ. Colorado

Page 11: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 11

New ZealandTectonic and bathymetric

setting

Image from NIWANational Institute of Water and Atmospheric Research Ltd

Central South Island experiences oblique continental collision at about 40 mm/yr

Shortening component normal to Alpine fault is about 10 mm/yr

Page 12: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 12

SAGENZ Profile: Karangarua to Lake Tekapo

MTJO

QUAR

Christchurch

Southern Alps Geodetic Experiment - New Zealand

Pacific Plate

Australian Plate

Image courtesy of Earth Sciences and Image Analysis Laboratory, NASA Johnson Space Center

40 mm

/yr

Page 13: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 13

OCCUPATION STRATEGY for CONTINUOUS and SEMI-CONTINUOUS GPS STATIONS

• Permanent ground marks at all sites, with force-centered antenna mounts

• Five sites occupied continuously, with data transmitted by radio modem and dial-up internet

• Six other sites occupied semi-continuously by rotating 3 receivers between the sites every 3 months

• 60-second sampling used to enable 3 months of data to be stored in internal memory

• Same antennas used at each site during each occupation

Page 14: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 14A Southern Alps semi-continuous GPS station

Page 15: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 15

Sometimes we have to find the sites

Page 16: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 16

And test snow integrity

Page 17: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 17

MTJO

CNCL

KARA

QUARNETT

MAKA

VEXA

WAKA

LEOC

PILK

REDD

Continuous station

Semi-continuous

SAGENZ GPS STATIONSA

lpin

e

Fau

ltNW SE

Image courtesy of Earth Sciences and Image Analysis Laboratory, NASA Johnson Space Center

Page 18: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 18

Vertical position time series after

filtering to remove annual signals and

common-mode noise

• RMS about a straight line fit is typically 2.5 - 4 mm. Worst case (NETT) is 6.5 mm.

Page 19: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 19Measured uplift rates and 95% confidence

Page 20: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 20

For a complete change in climate:Oil field monitoring in Oman.Summer daytime temperatures of 50C (120F)

Page 21: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 21

Basic GPS setupSite at the suspected center of the subsidence

Page 22: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 22

Continuous GPS site (5 of these)

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

GPS Monument and antenna

Passive cooled equipment box Telemetry antenna

Solar panelQuickTime™ and a

TIFF (Uncompressed) decompressorare needed to see this picture.

Drilled-braced monument

Page 23: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 23

Rover GPS sites (45 of these)

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

355 mm

Pillar is ~3 meters deep

Page 24: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 24

Time series of height estimates in the center of the field

Receiver failure and repair

Error bars scaled based on “global” GPS analysis

Two analysesshown that treatatmospheric delaydifferently

Page 25: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 25

Horizontalmotion at REM3

Note: if the sitewere truly at the center of the subsidence, no horizontal motion would be expected

Some non-steady motion can be seen

Page 26: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 26

Deformation from 9-months GPS

Page 27: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 27

Postglacial rebound in North America

• Here is combine temporal changes in position estimates from ~300 sites across North America.

• These results are generated by many different groups and need to be carefully evaluated.

• The results from the best sites are used to infer which GIA models best match the measurements. (Depends on structure of the Earth)

Page 28: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 28

Fit of COD to GIA: 9/1995-3/2004: 17 sites

This minimummoves with increasing LT

Lithosphere Thickness (LT) 71 kmDetails here depend geographic sites distribution

Page 29: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 29

Comparison of PUR solution (red, 50% confidence ellipses) with GIA model 71 km LT, UM 1, LM 2x1021 Pa-s

Fit: 26-sitesN 0.6 mm/yrE 0.3 mm/yrU 1.9 mm/yr

Page 30: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 30

Time series of Site GDAC for North and Height

Page 31: Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences 12.080 Seminar Fall 2004. tah

10/01/2004 12.080 GPS 31

Conclusions

• GPS dual-use technology: Applications in civilian world widespread– Geophysical studies (mm accuracy)– Engineering positioning (<cm in real-time)– Commercial positioning: cars, aircraft, boats (cm

to m level in real-time)• MIT has projects using GPS in many parts of the

world studying a variety of problems• Plate Boundary Observatory will be a major project

over the next 10 years in the US